The railway changed the town quickly. Its population stood at 1,244 in 1801 and 2,990 in 1841, inflated by around 800 railway labourers. Streets built in those years and soon after share a recognisable pattern, and so do their roof faults.
Q2.1Why do slates creep down a terrace roof?
A slate is nailed through two holes near its head and hangs from a batten. Once a nail corrodes, the slate creeps downhill, normally a little at a time, and water then gets through to the underlay. Swapping in a handful of slates is a quick job if the neighbouring ones are sound, but when slides keep appearing across a whole slope it is a sign the nails have failed generally and the slope needs re-fixing. Clay tiles fail differently, by laminating or cracking after frost, and they can be replaced one at a time.
Q2.2Why does the leak show up next door?
Terraces share chimney stacks, and every stack is a junction of brick, lead and slate. Flashing means the lead that seals that junction against rain, and a soaker is a small lead sheet worked into the slates beside the stack. When lead ages it splits along its folds. Water then runs down the stack into the party wall and shows up in a neighbour's ceiling. If a stack is disused, taking it down below the roofline is sometimes the cleanest answer, though taking out the chimney breast below always needs Building Regulations approval, and a breast on a shared wall brings in the Party Wall etc. Act.
Q2.3Could the valley be the real culprit?
Where two slopes meet at an inside corner, the valley carries a large share of the roof's water. A lead-lined valley that has split, or a valley clogged with moss, causes more ceiling stains than a missing slate. It is also the most overlooked part of the roof from the pavement.